The Atlantic's freshwater budget under climate change in the Community Earth System Model with strongly eddying oceans

We investigate the freshwater budget of the Atlantic and Arctic oceans in coupled climate change simulations with the Community Earth System Model and compare a strongly eddying setup with 0.1 ∘ ocean grid spacing to a non-eddying 1 ∘ configuration typical of Coupled Model Intercomparison Project ph...

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Published in:Ocean Science
Main Authors: A. Jüling, X. Zhang, D. Castellana, A. S. von der Heydt, H. A. Dijkstra
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2021
Subjects:
Online Access:https://doi.org/10.5194/os-17-729-2021
https://doaj.org/article/e3f6b1c4ffd24f63bfbca5226ef18acb
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author A. Jüling
X. Zhang
D. Castellana
A. S. von der Heydt
H. A. Dijkstra
author_facet A. Jüling
X. Zhang
D. Castellana
A. S. von der Heydt
H. A. Dijkstra
author_sort A. Jüling
collection Directory of Open Access Journals: DOAJ Articles
container_issue 3
container_start_page 729
container_title Ocean Science
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description We investigate the freshwater budget of the Atlantic and Arctic oceans in coupled climate change simulations with the Community Earth System Model and compare a strongly eddying setup with 0.1 ∘ ocean grid spacing to a non-eddying 1 ∘ configuration typical of Coupled Model Intercomparison Project phase 6 (CMIP6) models. Details of this budget are important to understand the evolution of the Atlantic Meridional Overturning Circulation (AMOC) under climate change. We find that the slowdown of the AMOC in the year 2100 under the increasing CO 2 concentrations of the Representative Concentration Pathway 8.5 (RCP8.5) scenario is almost identical between both simulations. Also, the surface freshwater fluxes are similar in their mean and trend under climate change in both simulations. While the basin-scale total freshwater transport is similar between the simulations, significant local differences exist. The high-ocean-resolution simulation exhibits significantly reduced ocean state biases, notably in the salt distribution, due to an improved circulation. Mesoscale eddies contribute considerably to the freshwater and salt transport, in particular at the boundaries of the subtropical and subpolar gyres. Both simulations start in the single equilibrium AMOC regime according to a commonly used AMOC stability indicator and evolve towards the multiple equilibrium regime under climate change, but only the high-resolution simulation enters it due to the reduced biases in the freshwater budget.
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Climate change
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Climate change
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spelling ftdoajarticles:oai:doaj.org/article:e3f6b1c4ffd24f63bfbca5226ef18acb 2025-01-16T20:40:40+00:00 The Atlantic's freshwater budget under climate change in the Community Earth System Model with strongly eddying oceans A. Jüling X. Zhang D. Castellana A. S. von der Heydt H. A. Dijkstra 2021-05-01T00:00:00Z https://doi.org/10.5194/os-17-729-2021 https://doaj.org/article/e3f6b1c4ffd24f63bfbca5226ef18acb EN eng Copernicus Publications https://os.copernicus.org/articles/17/729/2021/os-17-729-2021.pdf https://doaj.org/toc/1812-0784 https://doaj.org/toc/1812-0792 doi:10.5194/os-17-729-2021 1812-0784 1812-0792 https://doaj.org/article/e3f6b1c4ffd24f63bfbca5226ef18acb Ocean Science, Vol 17, Pp 729-754 (2021) Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2021 ftdoajarticles https://doi.org/10.5194/os-17-729-2021 2022-12-31T16:36:54Z We investigate the freshwater budget of the Atlantic and Arctic oceans in coupled climate change simulations with the Community Earth System Model and compare a strongly eddying setup with 0.1 ∘ ocean grid spacing to a non-eddying 1 ∘ configuration typical of Coupled Model Intercomparison Project phase 6 (CMIP6) models. Details of this budget are important to understand the evolution of the Atlantic Meridional Overturning Circulation (AMOC) under climate change. We find that the slowdown of the AMOC in the year 2100 under the increasing CO 2 concentrations of the Representative Concentration Pathway 8.5 (RCP8.5) scenario is almost identical between both simulations. Also, the surface freshwater fluxes are similar in their mean and trend under climate change in both simulations. While the basin-scale total freshwater transport is similar between the simulations, significant local differences exist. The high-ocean-resolution simulation exhibits significantly reduced ocean state biases, notably in the salt distribution, due to an improved circulation. Mesoscale eddies contribute considerably to the freshwater and salt transport, in particular at the boundaries of the subtropical and subpolar gyres. Both simulations start in the single equilibrium AMOC regime according to a commonly used AMOC stability indicator and evolve towards the multiple equilibrium regime under climate change, but only the high-resolution simulation enters it due to the reduced biases in the freshwater budget. Article in Journal/Newspaper Arctic Climate change Directory of Open Access Journals: DOAJ Articles Arctic Ocean Science 17 3 729 754
spellingShingle Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
A. Jüling
X. Zhang
D. Castellana
A. S. von der Heydt
H. A. Dijkstra
The Atlantic's freshwater budget under climate change in the Community Earth System Model with strongly eddying oceans
title The Atlantic's freshwater budget under climate change in the Community Earth System Model with strongly eddying oceans
title_full The Atlantic's freshwater budget under climate change in the Community Earth System Model with strongly eddying oceans
title_fullStr The Atlantic's freshwater budget under climate change in the Community Earth System Model with strongly eddying oceans
title_full_unstemmed The Atlantic's freshwater budget under climate change in the Community Earth System Model with strongly eddying oceans
title_short The Atlantic's freshwater budget under climate change in the Community Earth System Model with strongly eddying oceans
title_sort atlantic's freshwater budget under climate change in the community earth system model with strongly eddying oceans
topic Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
topic_facet Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
url https://doi.org/10.5194/os-17-729-2021
https://doaj.org/article/e3f6b1c4ffd24f63bfbca5226ef18acb